Sunday, April 28, 2019

Death Valley Field Trip- Mitchell Trenka


Death Valley Dunes




















These sand dunes are created by the weathering and erosion. Flash floods actually help send a lot of water rushing down mountain slopes grinding the rocks even more. This dune field includes three types of dunes: crescent, linear, and star shaped. And the highest dune is around 100 ft. My question is how does all this sand stay in the same area why aren’t their just bare rocks instead of all that sand staying in one place.







Racetrack Playa

This area is located on a very flat dry lake bed burrowed in-between two mountain ranges. This dry lake bed has flashes of life when heavy rain-washed water down from the surrounding mountains forming a very shallow lake. This water then evaporates and leaves that cracked texture you see in the pictures. The thing that makes this place so interesting is the mysterious moving of rocks in this lake bed. There are rocks that have slid as much at 2900 ft. Yet no person has every seen these rocks move. My question is where do the rocks that slide actually come from in the pictures, I have seen it doesn’t seem to have an abundance of rocks.

Split Cindercone

Less than 300,000 years ago magma filled a chamber underneath the earths crust. That magma began to rise up taking advantage of weaknesses found in the crust. Once it made its way out it created a fiery eruption sending molten basalt everywhere. Mu question is if this volcano is still active or has the chance to become active again. I also would like to know the rock types found around the cone.


Week 7, Field Trip Travel Journal: Death Valley - Jon Morris



Being from California, how could I resist the call to find out what Death Valley is all about.  I would guess that just about everyone that is native to California has heard about Death Valley, and it had a formidable name, but I had a desire to find out what it is about this region that caused it to be called Death Valley.  Being the curious person that I am, I decided to look into it.  I was somewhat surprised to find out that Death Valley was given its name by a group of pioneers that were lost there in the winter of 1849-1850.  The National Park Service let me know that although only one of the group of pioneers died there, they had all assumed that the valley would be their grave ("Frequently Asked Questions - Death Valley National Park (U.S. National Park Service)", 2018).

Once I had learned about the origin of the name, I just had to see it for myself and so I packed up the family and we travelled together to Death Valley National Park to check it out in person.  The first stop we made was to examine Titus Canyon.  Titus Canyon looks like it is a big gash cut into the Grapevine Mountains, as we can see from the below picture.  We found this interesting in light of our trip to the Grand Canyon last year.  We wondered if it was the same forces that cause this canyon, or rift, to form or if it was due to something else?  Based on what I understand about Geology, I would tend to assume that the Titus Canyon was formed by water somehow, but where is the water or where did the water come from?  I know that no river flows through it, so I believe that the canyon was formed with water from some source at some point in time, and I would like to figure out where the water came from that eroded this giant gash in the midst of the Grapevine Mountains.

Here is a picture of Titus Canyon taken by Marli Miller:










Credit:  Marli Miller.
















The second place we visited was called Dante’s View.  We learned that Dante’s View is on the north side of Coffin Peak, along the crest of the Black Mountains, overlooking Death Valley.  We learned that Dante’s View is a part of the Black Mountains, which is a part of the Amargosa Range, and was created when the surface of the Earth was being stretched, which ruptured the crust and caused lava to erupt over the sedimentary rock.  As we can see from the below picture, Dante’s View provides a truly unique view of what I would classify the “Basin” of Death Valley.  I know that the basin was created due to a stretching of the land, but I would like to know whether or not the stretching we can observe also resulted in any major faults?  Based on my personal visit and the pictures I was able to access, I am not able to determine whether or not there are any faults nearby or within the basin.

Here is a picture of Dante’s View taken by Marli Miller:

Credit:  Marli Miller.
















The final place we visited on our trip was called Zabriskie Point.  This was really a neat location where we were able to see, what for us, was a very unique example of geology.   Zabriskie Point overlooks what are commonly referred to as badlands.   Badlands are described as being a place where everywhere you see dry, finely-sculpted rock.  Looking at the below picture, one would almost think that it looked like it was covered in snow and ice.  I was able to find other pictures that make it appear more like what one would expect:  golden tan folds intersecting each other.  I have included the additional photo under the original photo from the travel guide.  Seeing all of the folds, it makes me wonder what it was that caused the folds?  I know that folds are caused through a variety and conglomeration of factors, such as stress, pressure, and temperature.  I do know that most folds are caused by compressional stress, so it would be interesting to see if that holds true in this case.  Was it strictly stress or pressure that caused these folds, or were there multiple factors that played into it?


Credit: Badlands topography. Photo by Paul Stone, USGS







Frequently Asked Questions - Death Valley National Park (U.S. National Park Service). (2018). Retrieved from https://www.nps.gov/deva/faqs.htm























Week 7- Death Valley

For week 7, we took a field trip to a place that has always been on my bucket list: The Death Valley. This place is so interesting to me because it is made up of so many different regions in one large area.  The region that really interested me the most was the Death Valley Dunes which are made up of the Cotton Wood Mountains that surround them on both sides. I think it is simple fascinating how sand starts out as a large rock and is crushed through a process by wind, rain, and tiny pieces of crushed rock overtime. It is interesting to me because it is so soft yet created by something hard and brittle. I had a few questions about wind storms, I have seen in movies people almost being swept away because they are so powerful, I want to learn more about them and also how they effect the beautiful sand ripples forming perfect patterns. 


Ripplemarks on Death Valley Dunes
















Death Valley Dunes

Frank, D. (n.d.). Death Valley geology field trip. Retrieved from https://geomaps.wr.usgs.gov/parks/deva/ftdune1.html

Week 7 Death Valley - Cobe Karhoff

Sinuous, water-sculpted curves of Mosaic Canyon marble
Mosaic Canyon

The first stop I visited was the Mosaic Canyon in Death Valley. As you can see in the photo, there are deep cuts in the mountain called Tucki Mountain. This canyon is made up of marble and the cuts are created from faults and also erosion. One question I have is how often does this canyon get eroded since Death Valley is a desert and rarely rains there.

Ubehebe and little Hebe craters
Ubehebe Crater
The second stop is Ubehebe Crater, which is considered a volcano at one point in time due to the thin layer of the crust allowing magma to seep through the faults and cracks on the crust. The question I would ask about this site is how often does this area get earthquakes? I never knew death valley had volcanoes located in the park, but now that I do know, I am curious to know how often earthquakes occur.


Polygonal cracks in salt pan
Badwater
My final stop is at Badwater, which is below sea level and the lowest point in the Western Hemisphere. The surface is made up of billions of crystals of almost pure table salt. The salt is created due to the dryness in the area and the salt is about 3-5 inches thick. My question about this stop is are there any volcanoes or any magma seeping through the crust since this area is below sea level.

Week 7- Field trip to Death Valley

Badlands topography


At the Badlands looking out from Zabriskie Point, with sediments of silt and clay create this beautiful effect that to me resembles waves. The multi color tops and and various sizes of these mounds brings me to the question: What is the average rain fall here? If is constant rain then it would have to cause a huge muddy mess? I would check the annual rain fall and then check how far the nearest town is to figure out how they prevent themselves or at all if flooding were to occur.
Shorelines etched into Shoreline Butte.

Shoreline Butte is the next stop we arrive to. The beautiful greenery and seeing the strandlines that are carved into the ground from the waves that once battered the shore. This brings me to a question of the history of all the lakes in the Death Valley thousands of years ago and how they have evaporated. How does the park keep them from getting filled back up? I would dive deeper into the Death Valley lakes and look at these on a topographic map to see the elevation and the surrounding around these lakes to get my answer.

Sinuous, water-sculpted curves of Mosaic Canyon marble

The last stop I would like to know more about is the Mosaic Canyon.The Sinuous, water sculpted curves of Mosaic Canyon marble. This place is breathtaking and I am in utter shock about how this canyon was formed millions of years ago. My question would be what type of fault is this canyon on for it to form the way it did millions of years ago? Would it change again if the fault that it was or still is on moves?


Week 7 - Meagan Valero

Mosaic Canyon
















I would like to start by visiting Mosaic Canyon. You can clearly see the different layers of strata deposited over time here. They seam to be fairly uniform in their color, which leads me to decide that the geological activity and types of rock being deposited over time must have been fairly consistent. I would like to know what process lifted or weathered down these rocks so the strata are visible, and whether or not that process is still occurring today.


Split Cinder Cone














Here we see split cinder cone. I wonder what process caused this region to be elevated above the surrounding area. As you can see, a fault line runs through the center of the cone. I would like to know what kind of fault this is, and whether it is caused by tension or compression.

Titus Mosaic
















Titus Mosaic is my favorite stop on the virtual tour. Here we see dark grey, angular rocks deposited in a sandy, light brown sediment. I wonder how these large grey rocks came to be composed differently than their surrounding sediment. I'd like to know exactly what the differences are between the makeup of the light grey sediment and the larger grey rocks so I can understand the various ways they formed.

Week 7 - Eric Valero

Artist's Pallet
My first stop is at Artist's pallet. Looking at these deposits, a number of colors are visible. I would want to know what minerals cause the color variations. I suspect that a number of salts and minerals are deposited by rains and flash flooding, but I can't know for sure what causes the coloration without studying the composition up close. It is interesting that these bright colors are at the base of a hill, which leads me to think that the water brings minerals from above down to mix at the base. I wonder why the colors aren't more prevalent at the top of the mountain if that's where the minerals come from.
Golden Canyon

Here at Golden Canyon we can clearly see stratified rock. I am curious as to if this rock was weathered by a stream in the area and if the stream is still present. There are obvious color variation between the strata near the top and strata at the bottom. I wonder what type of rock is near the base and why it is different from the rock near the top.
Mosaic Canyon
Here we see brightly colored, sharp rocks deposited among a sandy grey silt. I wonder how these sharp rocks got here, because most traveling rocks become more rounded by impacts over time. I also would like to know why they are so different from the surrounding silt, in order to explain the differences in color.